2.1. Formation of Mixed Structures
A distinct kind of phase behavior for the coadsorbed components
A and
B is the formation of ordered arrays with well-defined periodicity. This type of ordering results in a regular spatial arrangement of
A and
B, which can be advantageous, for instance, in creating reproducible 2D connections with emergent properties. Our simulations revealed that out of the 27 possible isomers of
B, only three were capable of exclusively forming extended mixed networks as dominant superstructures, that is,
1221,
1222,
2122, and
2132.
Figure 1 illustrates these networks, formed in an equimolar mixture of
A and
B, consisting of a total of 1600 molecules. Isomers
1222,
2122, and
2132 self-assembled into single mixed networks, while for unit
1221, two polymorphic structures,
12,
211 and
12212, were observed in the simulations. The latter polymorph was formed significantly less frequently, occurring in only 16 out of 50 system replicas. Networks
12211,
12212,
1222,
2122, and
2132 share similar properties, including a parallelogram shape and a 2
A + 2
B composition of the unit cell. Specifically, the dimensions of the unit cells are
,
;
,
;
,
;
,
; and
,
, respectively. Given the same composition of each unit cell, the differences in the density of the corresponding porous phases are influenced by the area of these cells so that
,
,
,
and
. Another common feature of the networks created by
1221,
1222,
2122, and
2132 is that they are heteroporous, consisting of three types of pores each. These void spaces are roughly deformed parallelograms (see the insets in
Figure 1), with rims defined by either 2
A + 2
B or 2
A + 4
B molecules. Interestingly, some of the pores are common to certain networks shown in
Figure 1. For example, the small 2
A + 2
B pores marked with orange dots are present in all the networks except for
1222, while the similar 2
A + 2
B pores indicated by blue dots are common to
12212,
1222,
2122, and
2132. Among these networks, the one formed by
1222 features the largest pores, encompassing 32 lattice sites.
The observed tendencies for pore formation can be explained based on the analysis of the interaction directions encoded in the considered tectons. To potentially create the medium-sized pores marked in blue, a B isomer must have two directional interactions 2 on either side (or both sides) of the linear core of this tecton. This implies that in the code abcd either or . Indeed, this condition is satisfied for 1222, 2122, and 2132, all of which form the aforementioned pores. Moreover, unit 1221 also meets the structural criterion described above and has been shown to form medium-sized cavities in the less abundant network polymorph denoted with subscript 2. Similarly, to create the small pores marked in orange, B has to be equipped with specific interaction directions assigned to a pair of arm segments connected to one end of the linear backbone. In this case, one direction should correspond to the para position, while the other should correspond to the meta position parallel to the core. This requirement can be met in several ways: and ; and ; and ; and and . Note that all of the B tectons satisfy one or more of these conditions, such as in the cases of 1221 and 2122, or in the case of 2132 (corresponding directions are underlined).
The specific sets of interaction directions in units
1221,
1222,
2122, and
2132 enabled the corresponding networks to propagate in the three principal directions of the lattice without defect formation. On the other hand, for the next two isomers,
2222 and
2231, the simulations produced extended mixed networks that lacked long-range order and contained numerous defects. The two bottom panels of
Figure 1 illustrate these molecular assemblies. In the case of
2231, a prominent structural feature of the corresponding network is the presence of local domains of
A, surrounded by double rows of
B, which glue and stabilize the entire architecture. However, numerous vacancy defects can be found there, with examples shown in the insets of the respective panels. These imperfections are primarily associated with the incomplete coordination of the tetrapod molecules (typically one or two; see the inset), which expose their dangling arms within the structural feature of the corresponding network in the presence of local domains of
A, surrounded by double rows of
B, which glue and stabilize the entire architecture. However, numerous vacancy defects can be found there, with examples shown in the insets of the respective panels. These imperfections are primarily associated with the incomplete coordination of the tetrapod molecules (typically one or two; see the inset), which expose their dangling arms within the pores. A somewhat different outcome of mixing was observed for tecton
2222, where the occlusion of
A domains was practically absent, and wide interconnecting rows of
B (and potentially
A) were not formed. As a result, components
A and
2222 were more widely dispersed within the network, leading to the observation of various defects, including the two largest shown in the pores. A somewhat different outcome of mixing was observed for tecton
2222, where the occlusion of
A domains was practically absent, and wide interconnecting rows of
B (and potentially
A) were not formed. As a result, components
A and
2222 were more widely dispersed within the network, leading to the observation of various defects, including the two largest shown in the inset next to the bottom right panel.
Regarding the relationship between the interaction directions of 2231 and 2222 and the morphology of the corresponding assemblies, some connections can be established. In the case of the first tecton, the formation of double molecular rows joining A domains is associated with the presence of two parallel interaction directions assigned to segments d and c of this tetrapod unit. This pair of parallel interaction directions (31) excludes the possibility of attaching two A molecules simultaneously. As a result, bimolecular complexes of 2231 are predominantly formed, and this basic structural motif is either incorporated into the rows or contributes to small fragments of a Kagome-like network of pure B, visible in the left part of the corresponding snapshot. For 2222, the significant structural complexity of the obtained network can be paradoxically associated with the high symmetry of this molecule. In this case, the centrosymmetric properties of 2222, with each interaction direction pointing along the arm, allow for a vast range of A–B configurations, leading to a multiverse of regular and deformed pores with undercoordinated molecules.
The final example of mixed structures created during all the simulation runs is the ladders comprising isomer 1331. Interestingly, we observed two polymorphic forms of these structures, I and II, differing in the relative arrangements of components A and B, shown in the respective inset. In one type of these ladders (I), pairs of molecules of A and pairs of molecules of 1331 were stacked alternately, parallel to each other and oriented perpendicular to the ladder growth direction. In the second type of ladders (II), the alternating pairs of tectons were tilted, and, furthermore, there was no direct contact between the molecules of A. The inability of isomer 1331 to co-assemble into extended networks primarily stems from the presence of interaction directions 1 and 3, which are associated with segments a and b. This pair of interaction directions gives isomer 1331 an anchor-like shape, and due to steric exclusion, when the ladder is formed, it allows for the attachment of molecules of A but not B. If two molecules of A are linked to 1331 in this manner, the structure can only grow in one direction, as the edge of the ladder becomes inactive with no exposed active segments.
The characteristic structural features of the self-assembled mixtures mentioned above are captured in the corresponding quantitative descriptors, one of which is the average number of molecule
B units coordinating with each molecule of
A,
CAB. This parameter approaches zero when separation occurs between
A and
B, and it is close to 3 when the components are perfectly mixed.
Figure 2 illustrates the changes in
CAB caused by decreasing temperature, as observed for the seven isomers shown in
Figure 1.
For the three tectons
1221,
2122, and
2132, the curves nearly overlap, indicating the formation of similar heteroporous periodic networks (see
Figure 1). The corresponding curves rise sharply as the temperature approaches approximately 0.23 and level off at a plateau close to 3. The sharp increase in
CAB signifies the condensation of the adsorbed components and the highly efficient incorporation of these units into the growing ordered domain. The contact value of
CAB (i.e., as
T → 0), which is approximately 3, confirms the previous common observation for the mixed networks containing
1221,
2122, and
2132, where each molecule of
A interacts with three neighboring molecules of
B. The slightly lower position of the plateau, just below 3, arises from the finite size of the porous domains, which include peripheral undercoordinated molecules of
A. For isomer
1222, the plateau of the coordination curve is significantly lowered to approximately 2, indicating that in the corresponding network, each molecule of
A coordinates with two molecules of
B.
The formation of ladders consisting of isomer 1331 resulted in a coordination curve that was less steep and reached a plateau lower than those of the network-forming tectons 1221, 2122, and 2132 (~3) but higher than that of 1222 (~2). In this case, the self-assembly of ladders occurred at somewhat higher temperatures, due to the increased stability of these emerging structures (for the ladders, disintegration can only begin at the ends, making it less efficient compared to the disintegration of network nuclei). The corresponding contact value of CAB, approximately 2.31, results from the different coordination patterns of A in the two types of ladders shown in the inset. In the case of ladders of type I, a molecule of A is in contact with two molecules of B, while for ladders of type II, it is fully coordinated by B. From an energetic perspective, the two types of ladders are identical, as each structure has every contributing molecule fully coordinated (except for the terminal ones). Consequently, the occurrence of ladders of type I and II should be equally probable, leading to a theoretical contact value of CAB = 2.5. The observed value of 2.31 is close to the theoretical prediction, and the difference arises mainly from the significant dispersion of ladders, which contain several undercoordinated molecules of A at the ends.
The irregular defective networks formed by
2222 and
2231 exhibit temperature dependencies that predict much lower heterogeneous coordination compared to the isomers discussed so far. Specifically, the obtained contact values of
CAB are equal to 1.32 and 1.05, respectively. These low values are a direct consequence of the clustering of components
A and
B in the networks depicted in
Figure 1. This effect results in the presence of numerous units of
A that have no interaction with
B—within the occluded
A fragments—and undercoordinated molecules of
A at the boundaries of these fragments, typically interacting with two units of
B. Thus, for both
2222 and
2231, the net average coordination of
A is close to 1, with the latter molecule exhibiting a stronger tendency to form occlusions;
CAB = 1.05. The shape of the corresponding curves shows that the
CAB(
T) calculated for
2231 is steeper, which may be attributed to the more efficient formation (condensation) of occluded
A domains. For
2222, the analogous curve indicates that the linkage of
A begins at higher temperatures, which can be attributed to the increased ease of forming mixed pores by the centrosymmetric
2222 unit. However, as previously mentioned, although the
2222 isomer can be more readily incorporated into the growing network and better mixed with
A, the resulting assembly remains highly disordered.
2.2. Segregation of Adsorbed Components
In this section, we discuss the qualitatively distinct self-assembly behavior of the adsorbed units
A and
B, which leads to their segregation. Specifically, we analyze representative examples of systems where various types of coexisting structures, composed solely of either
A or
B, were observed. The first type of phase behavior predicted for the given set of external parameters is the formation of a pure hexagonal network of
A [23], alongside a separate domain of single-type
B.
Figure 3 illustrates this effect for isomer
1113, which forms a densely packed brick-wall structure with a parallelogram unit cell of dimensions
and an angle of
. In the snapshot presented, additional, though very limited, stabilization of the domains is achieved through their direct contact. At the straight interphase boundary, molecules of
A and
B establish sparse interactions, with the latter primarily utilizing direction 1, which is assigned to segment
b. Due to the distinct periodicities of the contacting domains, these interactions occur between every second molecule of
A and every fourth molecule of
B, resulting in only a small contribution to the overall potential energy. The aforementioned segregation scenario was also observed for isomers
1213 and
1313, which formed structurally similar although more closely packed domains (see
Figure S2 of the Supporting Information section).
In contrast to the relatively dense phases formed by
1113,
1213, and
1313, the self-assembly of isomer
2131 resulted in a segregated hexagonal network with exceptionally large, regular pores, as shown in
Figure 3. This network features a large rhombic unit cell (
) with a side length of
, accommodating six molecules. A single hexagonal pore in the
2131 network encompasses 91 empty lattice sites, which is significantly larger compared to the hexagonal network of
A, where each pore spans only 19 lattice sites. Moreover, the pores formed by
2131 were identified as the largest among all the void spaces observed in this study. A periodic hexagonal network resembling that of
2131 was also formed by tecton
1112, featuring large pores spanning 67 lattice sites (see
Figure S2). A similar porous structure, albeit with smaller hexagonal void spaces consisting of 13 lattice sites, was observed for isomer
1111. In this case, the resulting network exhibited a Kagome topology and was characterized by a
unit cell with an angle of
, accommodating three molecules, as shown in
Figure 3.
A more complex segregation pattern of molecules
A and
B was associated with the coexistence of the pure
A network and one of the two possible polymorphs of
B-based networks. An example of the outcome of this segregation process is illustrated in the two bottom panels of
Figure 3, which depict isomer
2121. In this case, the molecules of
B formed either the Kagome (
k) network, characterized by large hexagonal pores, or the brick-wall network (
b), which features smaller parallelogram pores. The latter superstructure was less prevalent, appearing in 11 out of 50 system replicas. Networks
2121k and
2121b were characterized by unit cells of dimensions 7 by
(
) and
by
(
), respectively. The brick-wall network
2121b was frequently observed in contact with the porous domain of
A, as illustrated in the corresponding panel. For this type of network, similar to
1113, there was the possibility of forming a straight interface region where every second molecule of
A interacted with every fourth molecule of
B (utilizing direction
2 at segment
c). Although isomer
2121 exhibited a tendency to form more diverse structures, we never observed it mixing with
A during the simulations. The centrosymmetric molecules of
2121 were unable to intermix with
A, primarily due to the presence of interaction directions that were not collinear with their arms. These off-arm interactions hindered the extended growth of mixed networks, as the tripod molecules were unable to coordinate effectively with
B and form closed pores without vacancy defects. A similar segregation scenario, resulting in two polymorphic porous networks, was observed in the case of the
1121 isomer, as illustrated in
Figure S2. However, in this case, the alternative pure networks shared the same six-fold symmetry but differed in pore size.
In contrast to the relatively dense phases formed by
1113,
1213, and
1313, the self-assembly of isomer
2131 resulted in a segregated hexagonal network with exceptionally large, regular pores, as shown in
Figure 3. This network features a large rhombic unit cell (
) with a side length of
, accommodating six molecules. A single hexagonal pore in the
2131 network encompasses 91 empty lattice sites, which is significantly larger compared to the hexagonal network of
A, where each pore spans only 19 lattice sites. Moreover, the pores formed by
2131 were identified as the largest among all the void spaces observed in this study. A periodic hexagonal network resembling that of
2131 was also formed by tecton
1112, featuring large pores spanning 67 lattice sites (see
Figure S2). A similar porous structure, albeit with smaller hexagonal void spaces consisting of 13 lattice sites, was observed for isomer
1111. In this case, the resulting network exhibited a Kagome topology and was characterized by a
unit cell with an angle of
, accommodating three molecules, as shown in
Figure 3.
A more complex segregation pattern of molecules
A and
B was associated with the coexistence of the pure
A network and one of the two possible polymorphs of
B-based networks. An example of the outcome of this segregation process is illustrated in the two bottom panels of
Figure 3, which depict isomer
2121. In this case, the molecules of
B formed either the Kagome (
k) network, characterized by large hexagonal pores, or the brick-wall network (
b), which features smaller parallelogram pores. The latter superstructure was less prevalent, appearing in 11 out of 50 system replicas. Networks
2121k and
2121b were characterized by unit cells with dimensions of 7 by
(
) and
by
(
), respectively. The brick-wall network
2121b was frequently observed in contact with the porous domain of
A, as illustrated in the corresponding panel. For this type of network, similarly to
1113, there was the possibility of forming a straight interface region where every second molecule of
A interacted with every fourth molecule of
B (utilizing direction
2 at segment
c). Although isomer
2121 exhibited a tendency to form more diverse structures, we never observed it mixing with
A during the simulations. The centrosymmetric molecules of
2121 were unable to intermix with
A, primarily due to the presence of interaction directions that were not collinear with their arms. These off-arm interactions hindered the extended growth of mixed networks, as the tripod molecules were unable to coordinate effectively with
B and form closed pores without vacancy defects. A similar segregation scenario, resulting in two polymorphic porous networks, was observed in the case of the
1121 isomer, as illustrated in
Figure S2. However, in this case, the alternative pure networks shared the same six-fold symmetry but differed in pore size.
The last type of segregation refers to the formation of the
B-based structures with lower dimensions, such as chains and ladders. The growth of simple straight chains was observed for isomers
1212 and
1322, as illustrated in
Figure 3. This type of self-assembly of
B was also evident for tecton
3131, as shown in
Figure S2. In this context, it is worth noting that the self-assembly of chains was achievable for tectons where pairs of parallel interaction directions were positioned on opposite sides of tecton
B, either vertically or horizontally. Among the
27 isomers of B, only three possess this property: the centrosymmetric units
1212 and
3131, as well as isomer
1322, which exhibits a plane of symmetry. The complementary interaction directions assigned to pairs of segments located on opposite sides of the molecular core (
1212,
1322) or to segments connected to different parts of the core (
3131) dictate the directional growth of the corresponding chains. This type of linkage excludes the possibility of any bending or branching, resulting in straight chains that can grow along the three principal directions of the lattice.
Regarding ladder formation, such structures were observed in the case of isomer
1132 (
Figure 3), as well as for tectons
1231 and
1133 (c.f.
Figure S2). Depending on the assigned interaction pattern, the molecules within the ladders were either oriented along the propagation direction (
1132,
1133) or tilted by 60 degrees relative to it (
1231). Similarly to the chain-forming isomers, the self-assembly of ladders consistently produced straight structures, with the ends serving as the only growth points.
To understand the origin of the distinct segregation scenarios discussed above, let us take a closer look at the sets of interaction directions assigned to the corresponding tectons. In general, the formation of separate B-structures by certain isomers is primarily attributed to their inability to be fully or partially coordinated by A molecules, preventing the development of a unified molecular architecture. This situation is evident for B-tectons whose interaction directions are entirely incompatible with those of A in this regard. As mentioned earlier, the most straightforward example involves the chain-forming isomers 1212, 1322, and 3131, which are characterized by pairs of parallel interaction directions. For the remaining types of segregated B-structures, such general conclusions are much more difficult to draw and should be drawn with caution. For example, in the case of ladders, a potentially relevant feature of a tecton is the presence of parallel, oppositely oriented interaction directions on one side of the core, as takes place for 1132 and 1133. In these tectons, segments b and c are assigned the interaction directions 1 and 3, which align with the aforementioned criterion. The interaction between segments b and c of neighboring molecules facilitates the formation of a linear edge of the ladder, thereby stabilizing one strand. To connect a pair of strands, the tecton must be equipped with a complementary pair of interaction directions, allowing for the formation of arm-based rungs. For molecules 1132 and 1133, this is achieved through the pair of parallel and crossing interaction directions assigned to segments a and d, respectively. In the case of 1231, the edge-stabilizing interaction directions are assigned to a pair of segments (a and b) connected at one end of the core, while the strands are linked through a pair of parallel interaction directions assigned to the segments on the opposite side (c and d).
In summary, the necessary condition for a tecton B to create separated ladders can be formulated as follows: these isomers should possess a pair of parallel, oppositely directed interaction directions assigned to segments located on one side of the core or connected to one of its ends (edge-stabilizing directions). Furthermore, the interaction directions assigned to the remaining segments should be either parallel or crossing, and importantly, none of these directions can be parallel to the edge-stabilizing directions.
In the case of forming single networks containing B, the results obtained for isomer 1113 indicate that this type of phase separation is directly linked to the specific assignments of three interaction directions in this tecton. Specifically, to observe the densely packed brick-wall phase, a molecule of B should have a pair of crossing interaction directions on one side of the core (segments a and d). Moreover, this tecton must have one interaction direction that is opposite to the direction assigned to the diagonal arm segment (say c). Importantly, the interaction direction of the remaining segment (b) is irrelevant and can be assigned as 1, 2, or 3. This rule is supported by the results obtained from the simulations of the units 1213 and 1313, both of which formed brick-wall phases and differ from 1113 by the interaction direction assigned to the second position (b, underlined).
Regarding isomers 2131 and 1112 that formed the openwork hexagonal structures, certain similarities in the interaction patterns within these assemblies can be identified, providing the necessary conditions for the formation of network B with large pores to be formulated. Both molecules exhibit a pair of uniformly oriented interaction directions: in 1112, these directions are confined to one side of the molecular core, while in 2131, they are located on segments connected to one end of the core (underlined). When forming the network, a pair of 2131 (and similarly, 1112) molecules utilize these interactions to construct the pore rims. The remaining pair of interaction directions, which form a 60-degree angle relative to each other, are subsequently utilized to stabilize the triangular nodal motifs that serve as the vertices of the pores. The combination of these properties enables the formation of spacious void spaces, with their rims defined by pairs of molecules connected in a manner that maximizes the length of the connection.
Based on the results obtained for tecton
2121, it can be concluded that the occurrence of the two polymorphs shown in the bottom part of
Figure 3 is facilitated by parallel interaction directions associated with the diagonal arm segments. In this molecule, diagonal arm segments
a and
c have opposite interaction orientations (
2), while the same applies to segments
b and
d, which share a common but distinct orientation (
1). The assignment of distinct oppositely oriented interactions to pairs of diagonal segments, (
a,c) and (
b,
d), in
B proves to be a key factor, playing a similar role for the unit
1111 (also centrosymmetric), which is capable of forming the denser Kagome phase. An isomer worth mentioning here is
2222, which satisfies the above general condition but, unlike
1111 and
2121, here, mixes randomly with
B (see
Figure 1). This molecule, a prototype of various tetrapod molecular tectons (e.g., carboxylic acids) used in the experiment [
29,
30,
31], has previously been found to form both Kagome and brick-wall phases when adsorbed alone [
32]. The primary distinction between
2222 and the segregating units
1111 and
2121 lies in the fact that, in the former, all interaction directions are collinear with their respective arm segments. As this property significantly enhances the tendency of
2222 to mix with
A, the effect associated with pairs of oppositely oriented interactions in the diagonal segments, which is crucial for
1111 and
2121, is absent in this particular case.
The right part of
Figure 2 presents the heterogeneous coordination curves for the systems discussed in this section. Their shape is significantly different from the results characterizing systems where
A and
B formed mixed structures. The most notable feature of these dependencies is that
CAB drops nearly to zero when the temperature falls below approximately 0.2, indicating the complete resolution of adsorbed species. The common peaked shape of these curves reflects the initial formation of small mixed structures, followed by their breakdown and the growth of distinct, pure structures. Note that at maximum,
CAB does not exceed approximately 0.75, indicating very limited coordination of
A by
B at the transition temperature in each case. Thus, it can be concluded that the pure molecular assemblies grow effectively as separate entities, yet at elevated temperatures. Further lowering of
T finalizes this process by sorting out the residual units
A and
B for incorporation into the complementary extended structures. The less steep shape of the curves for
1212 and
1132 in the vicinity of the transition temperature (just above it) is associated with the formation of chains and ladders. In these cases, the growth process is more continuous due to the increased stability of multiple chains and ladder fragments, with only the end molecules being more likely to detach. A similar situation was previously observed for isomer
1331, which formed mixed ladders with
A (see the left part of
Figure 2). A noteworthy effect is the non-zero contact value
predicted for isomer
1322. This effect can be explained by the residual formation of mixed
A–
B chain fragments, as illustrated in the inset of the corresponding panel in
Figure 3. Although occurring much less frequently than the pure chains of
B, the mixed connections create local configurations where each molecule of
B interacts with two
A units. As a result,
CAB does not fully diminish to zero even at very low temperatures.
2.3. Complex Structure Formation
In the previous sections, we analyzed adsorbed systems where the dominant phase behavior involved the mixing or segregation of components A and B, resulting in more or less ordered assemblies. In the following, we consider those isomers of B for which simple classification was problematic due to the observed formation of both mixed and separated ordered networks, or disordered mixed assemblies with only traces of local ordering.
We begin the discussion with the most disordered and multiphase overlayers, represented by isomers
1123 and
1131, as shown in the top panels of
Figure 4. A clear effect observed for the first tecton is the segregation of a pure
A network within the disordered,
B-enriched mixture of the adsorbed species. The only indication of
B ordering in the latter assembly is the formation of sparse ladder-like structures, as shown in the corresponding inset. Importantly, these ladders are not fully energetically optimal structures, as each contributing
B unit forms only three interactions with its neighbors (indicated by yellow lines) and has one arm segment with an unpaired interaction direction (marked by red arrows). Nevertheless, in these structures,
1123 achieves the maximum possible coordination number of 3, which also characterizes the mixed portion of the assembly.
To demonstrate this, we calculated the temperature dependence of the fractions of molecules of
B interacting with 0 to 4 other molecules (both
A and
B), as shown in
Figure 5. A striking observation is the complete absence of fully coordinated
B molecules (with four interactions, orange curve) across the entire temperature range. When the temperature drops below approximately 0.25 and goes to zero, molecular condensation results in about 84% of molecules being triply coordinated and around 16% being doubly coordinated. In this final state, due to the specific interaction directions that strongly inhibit full coordination, the
1123 tecton utilizes its three arms in various configurations, leading to the formation of a mixed disordered domain and isolated, fragmented ladders. Similar phase behavior, with even more pronounced ladder formation, was observed for isomer
1223 (see
Figures S3 and S4). A possible explanation for the similar effects observed in
1123 and
1223 is the presence of crossing interaction directions on one side of the molecular core (specifically, the last two directions,
2 and
3), combined with a pair of non-parallel interaction directions on the opposite side.
The top-right section of
Figure 4 provides another example of a partially ordered system, where fragments of mixed porous phases were locally formed by
1131. The insets show magnified views of the porous networks, displaying honeycomb (
h) and brick-wall-type (1 and 2) topologies, respectively. The first two networks are 1:1 stoichiometric and are characterized by rhombic (
,
) and rectangular (
,
) unit cells. The third network, present in much smaller quantities, is a 2:1 (A:B) nonstoichiometric structure with a parallelogram unit cell (
,
). The unit cell of the hexagonal network with large pores consists of six molecules of
A and six molecules of
B, whereas the unit cells of brick-wall networks 1 and 2 contain two molecules of each type. The mixed networks formed locally by
1131 were observed frequently in the simulations (in different proportions) and reveal the increased tendency of this tecton for the easy formation of polymorphic structures with a 1:1 composition, which agrees with the overall proportions of
A and
B in the overlayer. This compositional match is a factor that ensures the equal consumption of molecules as they are incorporated into the growing equimolar networks. However, due to the diverse ways in which
1131 can be fully coordinated and form distinct (and also ordered) phases, these phases become highly competitive, leading to the complex morphology of the adsorbed mixture.
In the next example,
1122 demonstrates a dichotomous self-assembly scenario, resulting in either a pure disordered (aperiodic but continuous) domain of this tecton or a mixed superstructure with distinct periodic features, as illustrated in
Figure 4, with nearly equal probability. In the mixed domain, the molecules of
1122 form six-molecular clusters rotated by 60 degrees relative to one another. These differently oriented clusters are interconnected by molecules of
A, which are periodically arranged to form a hexagonal grid (see the red lines). The orientation of the
1122 clusters embedded in the network of
A is purely random (left or right), as the manner in which clusters of both types are linked to the network is identical. Consequently, this mixed architecture offers a higher degree of ordering for
1122 (though not fully periodic) compared to its pure segregated domain. In contrast to the previous isomer
1131, the composition of the mixed network is non-stoichiometric, with a proportion of
A to
B equal to 1:3.
The dichotomous manner in which the molecules of
A and
B can form adsorbed structures was also observed for isomers
1232 and
1321. In these instances, however, the self-assembly resulted in fully periodic 2D architectures, both for the segregation and mixing of the components.
Figure 4 illustrates this situation for
1321, while the results simulated for the other tecton are shown in
Figure S3 of the Supporting Information section. In the case of segregation, the molecules of
1321 self-assembled into a hexagonal network with spacious pores (43 sites) and a rhombic unit cell (
,
) consisting of six molecules of
A and six molecules of
B. The mixed, denser structure formed by this isomer is characterized by a parallelogram-shaped unit cell (
,
) with an equimolar composition (
2A +
2B). A defining feature of this superstructure is the presence of elongated pores, whose edges are formed of four molecules of each component.
The distinct self-assembly mechanisms of the
1122 and
1321 isomers are also evident in the corresponding coordination plots shown in the right panel of
Figure 5. In the case of segregation, the curves for both tectons are nearly identical, showing a distinct drop to zero at
T ≈ 0.25. This effect indicates the initial nucleation of molecules as the temperature decreases from 1 to 0.25, forming irregular connections with
A, followed by component self-sorting, where
A–
B contacts are almost entirely eliminated. Conversely, mixing in the examined systems results in temperature dependencies that differ significantly between
1122 and
1321. In this case, the initial nucleation of molecules at
T > 0.25 occurs similarly to segregation, with identical curves. However, at the transition temperature, the average coordination
CAB increases, reaching a plateau of approximately 1 for
1122 and 2 for
1321. The contact value for the latter molecule (
T → 0) has a more straightforward interpretation, as each
B molecule in the corresponding mixed domain is surrounded by two neighboring
A molecules. For
1321, the non-stoichiometric mixed 1:3 domain contains only one-third of the total number of
A molecules, while the remaining
A molecules form a pure honeycomb network. Each
A molecule in this one-third portion is connected to three
B units, while the remaining
A molecules in the pure network do not contribute to
CAB. As a result, the average heterogeneous coordination of
B is approximately 1. In the case of isomer
1232, the obtained temperature dependencies corresponding to segregation and mixing were very similar to those of
1321, as illustrated in
Figure S4.
Table 1 presents a summary of our results, categorizing them into mixed and segregated assemblies, along with more complex self-assembly scenarios. Additionally,
Table S1 provides the quantitative parameters of the ordered phases observed in the simulations. The grouping of isomers presented in
Table 1 can serve as a guide for the preliminary selection of tetrapod molecules to design 2D adsorbed structures with desired properties. Based on this information, molecular building blocks with various functional centers (atoms or groups) that enable directional interactions can be selected to construct superstructures sustained not only by weak intermolecular forces (e.g., hydrogen bonding) but also by covalent bonds. For example, when the considered model interaction centers are halogen atoms attached to a polyaromatic backbone of
B, the structures presented in our work can be useful for optimizing on-surface synthetic reactions, such as the Ullmann coupling. In this context, these theoretical predictions could have a potential impact on the design and fabrication of real, persistent, low-dimensional structures composed of mixtures of molecular tectons with different symmetries.